DELTIDIAL COVERINGS OF MIDDLE ORDOVICIAN CLITAMBONITIDINES (CLITAMBONITIDINA, BRACHIOPODA) AND THEIR SIGNIFICANCE FOR ATTACHMENT TO THE SUBSTRATE

dc.contributor.author	Madison A.A.
dc.date.accessioned	2022-11-04T07:50:43Z
dc.date.available	2022-11-04T07:50:43Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13468151
dc.identifier.citation	Paleontological Journal, 2004, 38, 6, 627-634
dc.identifier.issn	0031-0301
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/39467
dc.description.abstract	The growth and microstructure of deltidial covering plates of Lower and Middle Ordovician Clitambonitidines from Estonia and Leningrad Region are reviewed. In the genera Anchigonites, Antigonambonites, Vellamo, and Estlandia, the fusion of deltidial plates was followed by the formation of both the symphytium and the tube covering the pedicle. Subsequently, the end of the tube was sealed with the apical disc, which supposedly provided cementation to the substrate.
dc.subject	Clitambonitidina
dc.subject	Ordovician
dc.title	DELTIDIAL COVERINGS OF MIDDLE ORDOVICIAN CLITAMBONITIDINES (CLITAMBONITIDINA, BRACHIOPODA) AND THEIR SIGNIFICANCE FOR ATTACHMENT TO THE SUBSTRATE
dc.type	Статья
dc.subject.age	Paleozoic::Ordovician
dc.subject.age	Палеозой::Ордовикская	ru

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